Time domain reflectometry measurement principles and applications

被引:258
作者
Jones, SB [1 ]
Wraith, JM
Or, D
机构
[1] Utah State Univ, Dept Plants Soils & Biometeorol, Logan, UT 84322 USA
[2] Montana State Univ, Dept Land Resources & Environm Sci, Bozeman, MT 59717 USA
关键词
TDR; dielectric; permittivity; soil moisture; soil electrical conductivity;
D O I
10.1002/hyp.513
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Time domain reflectometry (TDR) is a highly accurate and automatable method for determination of porous media water content and electrical conductivity. Water content is inferred from the dielectric permittivity of the medium, whereas electrical conductivity is inferred from TDR signal attenuation. Empirical and dielectric mixing models are used to relate water content to measured dielectric permittivity. Clay and organic matter bind substantial amounts of water, such that measured bulk dielectric constant is reduced and the relationship with total water content requires individual calibration. A variety of TDR probe configurations provide users with site- and media-specific options. Advances in TDR technology and in other dielectric methods offer the promise not only for less expensive and more accurate tools for electrical determination of water and solute contents, but also a host or other properties such as specific surface area, and retention properties of porous media. Copyright (C) 2002 John Wiley Sons, Ltd.
引用
收藏
页码:141 / 153
页数:13
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